P. Heinrich et al., SIMULATION OF WATER-WAVES GENERATED BY A POTENTIAL DEBRIS AVALANCHE IN MONTSERRAT, LESSER-ANTILLES, Geophysical research letters, 25(19), 1998, pp. 3697-3700
The evolution of the volcano activity in Montserrat could lead to the
collapse of a portion of the lava dome in the Tar River Valley and to
a sudden entry of debris avalanche into the Caribbean Sea. The impact
of a debris avalanche with a volume of 40x10(6) m(3) into the sea and
the generated tsunami have been simulated numerically by a mixture mod
el solving the 3D Euler's equations. The mixture is composed of sedime
nts considered as an homogeneous fluid of density 2 and of water. Nume
rical tests show that the generated waves are sensitive to both initia
l impact velocities and avalanche fronts of the landslide. The water s
urface and velocities calculated by the 3D mixture model are used as i
nput data in a non-linear shallow water model, to calculate tsunami pr
opagation along the coasts of Montserrat. The hydraulic risks in Monts
errat are roughly assessed for a tsunami generated by a mass of 40x10(
6) m(3) entering the sea.